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Evidence for extensive post-Caledonian karst development in southwestern Spitsbergen

Published online by Cambridge University Press:  01 May 2009

M. Bjørnerud
M. Bjørnerud
Affiliation:
Geology Department, Miami University, Oxford, OH 45056–1618, U.S.A.
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Abstract

Proterozoic limestones at several localities in southwestern Spitsbergen contain karst-related features (layered clastic infillings, collapse breccias, deeply weathered depressions) which overprint the Caledonian deformational fabric in the rocks. These features apparently developedbetween middle Devonian and mid-Carboniferous time when the Precambrian basement complex stood high above sea level. Recognition of these karst features may shed light on depositional and tectonic events in post-Caledonian Spitsbergen.

Type
Articles
Information
Geological Magazine , Volume 129 , Issue 4 , July 1992 , pp. 465 - 469
Copyright
Copyright © Cambridge University Press 1992

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References

Birkenmajer, K. 1959. Report on the geological investigations of the Hornsund area, Vestspitsbergen, in 1958. I. The Hecla Hoek Formation. Bulletinde l' Académie Polonaise des Sciences VII, 129–36.Google Scholar
Birkenmajer, K. 1964. Devonian, Carboniferous and Permian formations of Hornsund, Vestspitsbergen. Studia Geologica Polonica 11, 47–123.Google Scholar
Challinor, A. 1967. The structure of Brøggerhalvøya, Spitsbergen. Geological Magazine 104, 322–36.CrossRefGoogle Scholar
Choquette, P. W. & James, N. P. 1988. Paleokarst: Introduction. In Paleokarst (eds James, N. P. and Choquette, P. W.), pp. 1–21. New York: Springer-Verlag.Google Scholar
Dallmann, W. 1990. Late Paleozoic tectonics in the Hornsund-Sørkapp area: New evidence of ‘Adriabukta phase’ deformation in basement mobile zone (abstract). Proceedings of Symposium on Post-Devonian Tectonic Evolution of Svalbard, 15–16 November, 1990, University of Oslo.Google Scholar
Dallmann, W. 1991. Multiphase tectonic evolution of the Sørkapp–Hornsund mobile zone (Devonian, Carboniferous, Tertiary), Svalbard. Norsk Geologisk Tidsskrift (in press).Google Scholar
Dallmann, W., Hjelle, A., OHTA, Y., Salvigsen, O., Bjørnerud, M., Maher, H., Hauser, E. & Craddock, C. 1990. Geological map of Svalbard (1.100,000), Sheet BIIG: Van Keulenfjorden. Norsk Polarinstitutt Temakart no. 15, 58 pp.Google Scholar
Dallmann, W & Maher, H. 1989. The Supanberget area - basement imbrication and detached foreland thrusting in the Tertiary fold-and-thrust belt, Svalbard. Polar Research 7, 95–107.Google Scholar
Flood, B., Nagy, J. & Winsnes, T. S. 1971. Geological map of Svalbard (1:500,000) Sheet 1G, southern part. Norsk Polarinstitutt Skrifter no. 154 A.Google Scholar
Ford, D. 1988. Characteristics of dissolutional cave systems in carbonate rocks. In Paleokarst (eds James, N. P. and Choquette, P. W.), pp. 25–57. New York: Springer-Verlag.CrossRefGoogle Scholar
Gjelberg, J. G. & Steel, R. 1981. An outline of Lower-Middle Carboniferous sedimentation on Svalbard. In Geology of the North Atlantic Borderlands (eds Kerr, J. M. and Ferguson, A.J.), pp. 543–61. Canadian Society of Petroleum Geologists Memoir no. 7.Google Scholar
Harland, W. B., Cutbill, J. L., Friend, P. F., Gobbett, D. J., Holliday, D. W., Maton, P. I., Parker, J. I. & Wallis, R. H. 1974. The Billefjorden Fault Zone, Spitsbergen: The long history of a major tectonic lineament. Norsk Polarinstitutt Skrifter no. 161, 72 pp.Google Scholar
Harland, W. B., Gaskell, B. A., Heafford, A. P., Lind, E. K. & Perkins, P. J. 1984. Outline of Arctic post-Silurian continental displacements. In Petroleum Geology of the North European Margin (ed. Spencer, A. M.), pp. 137–48. London: Graham & Trotman.CrossRefGoogle Scholar
Hjelle, A. & Lauritzen, Ø. 1982. Geological map of Svalbard (1:500,000), sheet 3G, Northern part. Norsk Polarinstitutt Skrifter no. 154C, 15 pp.Google Scholar
Lamar, D., Reed, W. & Douglass, D. 1986. Billefjorden fault zone, Spitsbergen: Is it part of a major late Devonian transform? Geological Society of America Bulletin 97, 1083–8.2.0.CO;2>CrossRefGoogle Scholar
Mann, A. & Townsend, C. 1989. The post-Devonian tectonic evolution of southern Spitsbergen illustrated by structural cross-sections through Bellsund and Hornsund. Geological Magazine 126, 549–66.CrossRefGoogle Scholar
Steel, R. J. & Worsley, D. 1984. Svalbard's post-Caledonian strata - an atlas of sedimentary patterns and paleogeographic evolution. In Petroleum Geology of the North European Margin (ed. Spencer, A. M.), pp. 109–35. London: Graham & Trotman.CrossRefGoogle Scholar
Torsvik, T., Løvlie, R. & Sturt, B. 1985. Paleomagnetic argumentfor a stationary Spitsbergen relative to the British Isles since late Devonian time. Earth and Planetary Science Letters 75, 278–88.CrossRefGoogle Scholar
Worsley, D. & Aga, O. J. 1986. The Geological History of Svalbard. Stavanger: Den Norske Stats Oljeselskap, 121 pp.Google Scholar